Orthoclase: Difference between revisions

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'''Orthoclase,''' or '''orthoclase [[feldspar]]''' ([[endmember]] formula [[potassium|K]][[aluminium|Al]][[silicon|Si]]<sub>3</sub>[[oxygen|O]]<sub>8</sub>), is an important [[Silicate minerals#Tectosilicates|tectosilicate]] [[mineral]] which forms [[igneous rock]]. The name is from the [[Ancient Greek]] for "straight fracture", because its two cleavage planes are at right angles to each other. It is a type of '''potassium feldspar''', also known as '''K-feldspar'''. The gem known as [[Moonstone (gemstone)|moonstone]] (see below) is largely composed of orthoclase.
 
==Formation and subtypes==
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==Uses==
Together with the other potassium [[feldspar]]sfeldspars, orthoclase is a common raw material for the manufacture of some [[glass]]es and some [[ceramic]]s such as [[porcelain]], and as a constituent of scouring powder.
 
Some intergrowths of orthoclase and [[albite]] have an attractive pale [[luster (mineralogy)|luster]] and are called [[Moonstone (gemstone)|moonstone]] when used in jewellery. Most moonstones are translucent and white, although grey and peach-colored varieties also occur. In gemology, their luster is called [[adularescence]] and is typically described as creamy or silvery white with a "billowy" quality. It is the [[state gem]] of [[Florida]].